Kame or Moraine? A Sedimentological Study of a Glaciomarginal Landform at Niedźwiedziny (Great Polish Lowland)
A sedimentary succession in a gravel pit at Niedźwiedziny was investigated in order to determine its origin: kame or moraine. The gravel pit is located in an isolated hill of approx. 600 m long and 250–400 m wide.
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| Format: | Article |
| Language: | English |
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Sciendo
2014-10-01
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| Series: | Geologos |
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| Online Access: | http://www.degruyter.com/view/j/logos.2014.20.issue-3/logos-2014-0013/logos-2014-0013.xml?format=INT |